Petrography: The meteorite shows a chondritic texture of abundant small chondrules, metals, sulfides, CAIs, and mineral fragments embedded into a fine-grained greyish and porous matrix. Chondrules are dominantly porphyritic and typically 0.1-0.2 mm in diameter. Sulfides and FeNi metal are fresh and present in matrix and chondrules.

Classification: The textural observations suggest a CO3 classification of this rock. The olivines show undulatory extinction. Thus, the rock is of shock stage S2. The sample is only slightly weathered.